Seasonal thermohaline fluctuations in the middle Adriatic Sea (

Seasonal thermohaline fluctuations in the middle Adriatic Sea (
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亚得里亚海中部的季节性温盐波动（

DOI：
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发表时间：
1997
期刊：
影响因子：
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通讯作者：
M. Morovic
M. Morovic
中科院分区：
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文献类型：
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作者：
B. Grbec;M. Morovic

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分析了1961-1980年亚得里亚海中部Split-Gargano断面的公海站的盐度和温度时间序列。温盐波动用基本原理来描述 此外，还与海-气界面的热通量和水通量进行了比较。近地层温度和盐度垂直梯度与全年的地表通量有很好的相关性。在更深层，这种影响只有在垂直均匀的条件下才可见。热量和盐分的垂直通量与热量和盐分含量的变化率相比，表明季节具有重要的平流效应。冷季以垂直交换为主，暖期以水平交换为主。
Salinity and temperature time series were analysed for the open sea stations at the transect Split-Gargano, in the middle Adriatic, for the period 1961-1980. Thermohaline fluctuations were described in terms of the principal component scores and, in addition, were compared to heat and water flux at the atmosphere-sea interface. Temperature and salinity vertical gradients in the surface layer are well related to surface fluxes during the whole year. In deeper layers this influence is visible only under the vertically homogenous conditions. Vertical fluxes of heat and salt, compared to the rate of change of the heat and salt content, point to the season with important advection effects. Vertical exchange prevails in the cold season, while horizontal exchange is considerable in the warm period.